High and Low Pressure Cells
Learn how Highs and Lows differ in pressure, vertical air movement and surface circulation, and why each brings the weather it does.
Understand how berg winds warm and dry the coast, why cities build their own heat island, and how a valley inversion traps the air we breathe.
By the end, you can
explain berg wind warming, urban heat islands and why pollution becomes trapped under an inversion.
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Berg Winds, Heat Islands and Urban Air
Hot air in the wrong season
A winter day on the KwaZulu-Natal or Eastern Cape coast turns unexpectedly hot and dry. The humidity drops, the wind comes off the land instead of the sea, and the fire danger rating climbs. That is a berg wind. 🔥
Then there is the other side of it: a city that stays warmer than the farmland around it, and a valley that holds its own exhaust fumes on a still morning. All three are the same physics seen in different places.
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Next on the Geography path · step 4 of 11
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Learn how Highs and Lows differ in pressure, vertical air movement and surface circulation, and why each brings the weather it does.
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Berg Winds, Heat Islands and Urban Air
R19 · 12 min · certificate